EGU24-2007, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-2007
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Modelling post-restoration spatiotemporal changes in peatland water table with optical satellite imagery

Aleksi Isoaho1,2, Lauri Ikkala2,3, Lassi Päkkilä2, Hannu Marttila2, Santtu Kareksela4, and Aleksi Räsänen1,5
Aleksi Isoaho et al.
  • 1Natural Resources Institute Finland, Oulu, Finland (aleksi.isoaho@luke.fi)
  • 2Water, Energy and Environmental Engineering Research Unit, University of Oulu, Oulu, Finland
  • 3Geological Survey of Finland, Kokkola, Finland
  • 4Metsähallitus Parks & Wildlife Finland, Hämeenlinna, Finland
  • 5Geography Research Unit, University of Oulu, Finland

Remote sensing (RS) has been suggested as a tool for peatland monitoring. However, there have been only a few studies in which post-restoration hydrological changes have been quantified with RS-based modelling. To address this gap, we developed an approach to assess post-restoration spatiotemporal changes in the peatland water table (WT) with optical Sentinel-2 and Landsat imagery. We tested the approach in eleven northern boreal peatlands (six restored, and five control sites) impacted by forestry drainage in northern Finland using Google Earth Engine cloud computing capabilities. We constructed a random forest regression model with spatiotemporal field-measured WT data as a dependent variable and satellite imagery features as independent variables. To assess the spatiotemporal changes, we constructed representative maps for situations before and after restoration, separately for early summer wet and midsummer dry conditions. To further quantify temporal changes during 2013–2023, and to test statistical significance of restoration, we conducted a bootstrap hypothesis test for the areas near the restoration measures and similar areas in the control sites. The regression model had a relatively good fit and explanatory capacity (R2 = 0.61, RMSE = 6.98 cm). The WT maps showed that the post-restoration changes were not uniform and concentrated near the restoration measures. The bootstrap test showed that the WT increased more in the restored areas (5.8–9.4 cm) than in the control areas (0.1–4.5 cm). Our results indicate that restoration impact on surface hydrology can be quantified with optical satellite imagery and a machine learning approach in treeless peatlands.

How to cite: Isoaho, A., Ikkala, L., Päkkilä, L., Marttila, H., Kareksela, S., and Räsänen, A.: Modelling post-restoration spatiotemporal changes in peatland water table with optical satellite imagery, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-2007, https://doi.org/10.5194/egusphere-egu24-2007, 2024.